Talk:Climate of ancient Rome: Difference between revisions

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Revision as of 19:10, 26 August 2014 editBrandmeister (talk \| contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers38,017 edits ←Created page with '{{WikiProject Classical Greece and Rome}} {{WikiProject Environment\|climate change=yes}}'		Revision as of 07:58, 30 November 2014 edit undoWilliam M. Connolley (talk \| contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers, Rollbackers66,021 edits →Evidence for a cooler Mediterranean climate...: new sectionNext edit →
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			== Evidence for a cooler Mediterranean climate... ==

			This

			: ''Evidence for a cooler Mediterranean climate in 600 BC–100 BC comes from remains of ancient harbors at Naples and in the Adriatic which are located about one meter below current water level''

			makes no sense. Local climate doesn't affect sea level. Also http://www.researchgate.net/publication/222837315_Sea_level_in_Roman_time_in_the_Central_Mediterranean_and_implications_for_recent_change/links/0c96051dc446a4d29f000000 says ''These data provide a precise measure of local sea level of � 1.35 F 0.07 m at 2000 years ago. Part of this change is the result of ongoing glacio-hydro isostatic adjustment of the crust subsequent to the last deglaciation. When corrected for this, using geologically constrained model predictions, the change in eustatic sea level since the Roman Period is � 0.13 F 0.09 m'' ] (]) 07:58, 30 November 2014 (UTC)

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Evidence for a cooler Mediterranean climate...

This

Evidence for a cooler Mediterranean climate in 600 BC–100 BC comes from remains of ancient harbors at Naples and in the Adriatic which are located about one meter below current water level

makes no sense. Local climate doesn't affect sea level. Also http://www.researchgate.net/publication/222837315_Sea_level_in_Roman_time_in_the_Central_Mediterranean_and_implications_for_recent_change/links/0c96051dc446a4d29f000000 says These data provide a precise measure of local sea level of � 1.35 F 0.07 m at 2000 years ago. Part of this change is the result of ongoing glacio-hydro isostatic adjustment of the crust subsequent to the last deglaciation. When corrected for this, using geologically constrained model predictions, the change in eustatic sea level since the Roman Period is � 0.13 F 0.09 m William M. Connolley (talk) 07:58, 30 November 2014 (UTC)

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